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1 Application of Weighted Essentially Non-Oscillatory Limiting to Compact Interpolation Schemes Debojyoti Ghosh Graduate Research Assistant Alfred Gessow.

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Presentation on theme: "1 Application of Weighted Essentially Non-Oscillatory Limiting to Compact Interpolation Schemes Debojyoti Ghosh Graduate Research Assistant Alfred Gessow."— Presentation transcript:

1 1 Application of Weighted Essentially Non-Oscillatory Limiting to Compact Interpolation Schemes Debojyoti Ghosh Graduate Research Assistant Alfred Gessow Rotorcraft Center Aerospace Engineering Department University of Maryland, College Park AIAA Region I Young Professional, Student, and Education Conference 2011 4 th November, 2011, Johns Hopkins University / Applied Physics Laboratory Kossiakoff Center, Laurel, MD James D. Baeder Associate Professor

2 2 Motivation and Objectives Accurate numerical simulation of the wake flow field around a rotorcraft –Long term convection and mutual interaction of vortices –Interactions of vortices with fuselage and ground plane High order accurate Navier- Stokes solver –Lower dissipation to preserve vortices as they convect over large distances –Smaller stencil for same order of accuracy to reduce data transfer costs for multiple-mesh solutions

3 3 Introduction Scalar hyperbolic partial differential equation Discretization in time leads to an ordinary differential equation (solved by Euler explicit or TVD RK3) Reconstruction – interpolation of f at the interfaces from the cell centered/averaged values Upwinding – biased interpolation stencil to model wave nature of the solution

4 4 Compact Schemes High order accuracy with smaller stencils Better spectral resolution than explicit interpolation Lower dissipation at well-resolved frequencies Taylor series error order of magnitude lower

5 5 Compact-Reconstruction WENO Schemes Convex combination of candidate r-th order accurate stencils Weights of each stencil based on “smoothness” (measured by divided differences of the appropriate order) Traditional WENO schemes use explicit interpolation –Higher order accuracy  wider stencil  oscillatory solutions Compact-Reconstruction (CRWENO) schemes constructed by using implicit interpolations as candidates in the WENO algorithm –Advantages of compact interpolation schemes (smaller stencil, lower dispersion and dissipation, lower absolute errors) –Non-oscillatory reconstruction across discontinuities Optimal Weights WENO Weights

6 6 Example: CRWENO5

7 7 Smoothness Indicators Weights are calculated based on smoothness indicators of corresponding explicit stencils (same as WENO5 scheme)

8 8 Linear Advection Equation 5 th order convergence with lower absolute error than WENO5 Less smearing and clipping than WENO5

9 9 Inviscid Burgers Equation Initial sinusoidal solution turns into a shock wave (non-linear flux) 5 th order convergence (before shock formation) with lower absolute error than WENO5

10 10 Extension to the Euler Equations Compressible Euler equations in 1D given by In the form of a general hyperbolic PDE Extension of interpolation schemes for scalar quantities to a system of equations –Component-wise reconstruction of conservative variables (ρ, ρu, e) –Reconstruction of primitive (flow) variables (ρ, u, p) –Reconstruction of characteristic variables

11 11 Characteristic-based Reconstruction Characteristic based reconstruction respects the physics of the problem – 1D scalar wave propagation along each characteristic i i+1 U avg (Roe averaged) Eigenvalues, left and right eigenvectors For interface j+1/2, characteristic quantities are given by Reconstruct Upwinding (Roe-Fixed) Flux in conservative form

12 12 CRWENO5 for 1D Euler Equations Scalar interpolation scheme applied to the characteristic variables Results in a block tri-diagonal linear system along each dimension (as compared to tri-diagonal system for component-wise reconstruction) For multi-dimensions, solution of linear system required along each grid line k = 1,2,3

13 13 Entropy Wave Smooth problem involving the convection of an entropy wave –Density wave convects without dissipation, constant velocity and pressure Exact solution given by Periodic boundary conditions enforced on both boundaries Solution compared after one pass over the domain Errors and order of convergence compared –Lower absolute errors for CRWENO5 at same order of convergence

14 14 1D Riemann Problems Initial condition consists of two states separated by a thin partition Initial discontinuity is decomposed into a rarefaction wave (RF), a contact discontinuity (CD) and a shock wave (S) –Sod’s shock tube problem –Lax’s shock tube problem Benchmark cases for code validation Require robust solvers to prevent spurious oscillations RFCDS

15 15 Sod’s Shock Tube Comparison of different reconstruction methods Comparison of WENO5 and CRWENO5 Characteristic – based reconstruction yields non-oscillatory results (though computationally more expensive) Low dissipation of CRWENO5 results in sharper resolution of shock and contact discontinuity

16 16 Lax’s Shock Tube Oscillations caused by reconstruction of conservative and primitive variables CRWENO5 shows less smearing of shock and contact discontinuity Conservative Variable Reconstruction Characteristic-based Reconstruction

17 17 Shock-Entropy Interaction Interaction between a shock wave and an entropy wave –Solution contains discontinuity and high-frequency waves Initial condition consists of right-moving shock and density wave Extrapolation boundary conditions enforced on both boundaries “Fine Grid Solution” obtained with WENO5 on 2000 point grid CRWENO shows lower dissipation and clipping of high- frequency waves

18 18 Isentropic Vortex Convection (Euler 2D) Convection of an isentropic vortex on a periodic domain Results shown for a 40x40 grid with WENO5 and CRWENO5 Lower dissipation of CRWENO5 preserves vortex for long–term convection Y-Velocity after 1 cycles over the domain Pressure after 1 and 5 cycles over the domain

19 19 Conclusions and Future Work Benefits of using the Compact-Reconstruction WENO scheme –Smaller stencil for same order of convergence, lower absolute errors –Lower dissipation leads to better resolution of discontinuities and better long-term convection properties –Computational expense at same grid size is marginally more but coarser grids can be used for same error in solution Characteristic vs. Component-wise reconstruction –Characteristic reconstruction is costlier, even more so for implicit reconstruction schemes (block tri-diagonal solver) –More robust since physically more accurate – non-oscillatory results for sharp discontinuities –Results similar in case of smooth flows Implementation of CRWENO for multi-dimensions –2D and 3D Navier-Stokes solvers –Application to airfoil cases, including pitching and plunging airfoils –Simulation of flow field in a rotorcraft wake (convection and interaction of wake vortices)

20 20 End


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